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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Descent from the polar mesosphere and anomalously high stratopause observed in 8 years of water vapor and temperature satellite observations by the Odin Sub-Millimeter Radiometer
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Descent from the polar mesosphere and anomalously high stratopause observed in 8 years of water vapor and temperature satellite observations by the Odin Sub-Millimeter Radiometer

机译:Odin亚毫米辐射仪在8年的水汽和温度卫星观测中观测到极地中层的下降和异常的高平顶层

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摘要

Using newly analyzed mesospheric water vapor and temperature observations from the Sub-Millimeter Radiometer instrument aboard the Odin research satellite over the period 2001-2009, we present evidence for an anomalously strong descent of dry mesospheric air from the lower mesosphere into the upper stratosphere in the winters of 2004, 2006, and 2009. In the three cases, the descent follows the recovery of the upper stratospheric polar vortex from a major midwinter stratospheric sudden warming. It is also accompanied by the rapid formation of an anomalously warm polar mesospheric layer, i.e., an elevated polar stratopause, near 75 km, and its slower descent to prewarming level (near 1 hPa) over 1.5-2 months. These three winters stand out in the current record of Odin/Sub-Millimeter Radiometer observations started in July 2001.
机译:利用新分析的Odin研究卫星在2001-2009年期间从亚毫米辐射计仪器获得的中层水汽和温度观测结果,我们提供了干燥中层空气异常异常强烈地从低层中层大气下降到平流层上层的证据。 2004年,2006年和2009年的冬季。在这三种情况下,下降是由于平流层中部一次冬季突然暖化而恢复了平流层上极涡旋。它还伴有异常温暖的极地中层异常层的迅速形成,即在75 km附近极地平顶层升高,并且在1.5-2个月内下降到预热水平(接近1 hPa)。这三个冬天在2001年7月开始的Odin /次毫米辐射计观测记录中脱颖而出。

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